GP51B-3721:
Large-scale geometry and temporal variability of the Martian external magnetic field
Large-scale geometry and temporal variability of the Martian external magnetic field
Abstract:
The martian magnetic field is unique among the terrestrial planets, as it resultsfrom the interaction of fields caused by crustal remnant magnetization and a planetary
ionosphere with the solar wind and the interplanetary magnetic field. Internal fields of
crustal origin have been subject to extensive studies, whereas the focus of our work deals
with average spatial structure and time variability in the martian external magnetic field.
We use the Mars Global Surveyor (MGS) vector magnetic field data to investigate the
large-scale geometry and magnitude of such external fields. We analyze the day-time and
night-time magnetic signature for the duration of the MGS mission in mapping orbit
(2000-2006). We use along-track vector field measurements to estimate the day-time
and night-time external fields after the subtraction of predicted crustal magnetic fields
at spacecraft altitudes. We also examine day/night differences (i.e., the daily variation)
in external fields; these are independent of crustal fields. Because the external fields are
modified by the crustal fields, we investigate their structure as a function of latitude in
the local time frame and as a function of both latitude and longitude in the body-fixed
frame. In the body-fixed-frame BΘ is generally dominant in magnitude with a day/night
variation described to first order by a zonal degree-2 spherical harmonic structure.
Br is strongly correlated with the crustal magnetic field. BΦ shows variable spatial
behaviour during both night and day. Seasonal variations are observed as stronger
average magnetic fields in the hemisphere pointing towards the sun. Additional shorter
time scale variations in the global external field structure are observed.